Along the Wuzunxiao segment, the left lateral dislocation landform is well developed.
乌尊硝段左旋走滑的断错地貌极为发育。
The opposite rotation direction implies the existence of left lateral dislocation between Qaidam basin and Jiuquan and Subei areas.
柴达木盆地和酒泉、肃北旋转方向的差异预示了两地区间存在左旋错动。
The normal fault zone with NEE trending are cut by some NNW faults with left-lateral dislocation in the north of the basin.
盆地北缘的北东东向正断层被北北西向断裂左旋错动。
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